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首页> 外文期刊>Current Journal of Applied Science and Technology >Dar Zarrouk Parameters for Delineation ofGroundwater Potential Zones in Geriyo IrrigationFloodplain of River Benue, Adamawa State,Northeastern Nigeria
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Dar Zarrouk Parameters for Delineation ofGroundwater Potential Zones in Geriyo IrrigationFloodplain of River Benue, Adamawa State,Northeastern Nigeria

机译:尼日利亚东北部阿达玛瓦州贝努河河平原上的Dar Zarrouk参数用于划定Geriyo灌溉区的地下水位

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摘要

The study is aimed at delineating groundwater potential zones of the alluvial formations using Dar Zarrouk Parameters and groundwater flow direction on the floodplain. This will help the farmers to utilise the floodplain shallow wells during the dry season farming. Shallow wells on the floodplain of River Benue are the primary sources of water supply for irrigation activities. The floodplain is underlain by Bima sand stones. Twenty-four profiles of vertical electric soundings using Schlumberger array method with the aid of a sensitive ABEM Signal Averaging System (SAS) was used to investigate. The results were then compared with the alluvial floodplain lithologies at each sounding points with resistivity values ranging between 0.146 Ωm to 9,873.6 Ωm and depths varying from 0.2 to 38.33 m. The geoelectric sequence of the alluvial formations of the floodplain reveals semi aquifer system. The aquifer hydraulic characteristics indicated that the transverse resistance, R ranged between 2,626.70 Ωm~(2) to 241,252.38 Ωm~(2) with a mean value of 45,172.17 Ωm~(2). The longitudinal conductance, S ranged between 0.001 to 0.221 with an average value of 0.036. The hydraulic conductivity value across the floodplain ranges between 0.21 m/day to 29.06 m/day with a mean value of 11.22 m~(2)/day. The transmissivity values obtained for the various layers ranges between 1.68 m~(2)/day to 808.16 m~(2)/day with an average value of 214.07 m~(2)/day. Three groundwater potential zones were delineated on the floodplain. The results of the hydraulic head reveal that the water levels in the floodplain are higher than the River and recharge the River.
机译:这项研究的目的是使用Dar Zarrouk参数和洪泛区的地下水流向来描绘冲积层的地下水潜在区域。这将有助于农民在旱季种植期间利用洪泛区浅井。贝努河河漫滩上的浅井是灌溉活动的主要水源。泛滥平原上有比马砂岩。使用Schlumberger阵列方法和灵敏的ABEM信号平均系统(SAS),研究了垂直电测深的二十四个剖面。然后将结果与每个探测点的冲积洪泛平原岩性进行比较,其电阻率值在0.146Ωm至9,873.6Ωm之间,深度在0.2至38.33 m之间。洪泛区冲积层的地电序列揭示了半含水系统。含水层的水力特性表明,横向阻力R在2,626.70Ωm〜(2)至241,252.38Ωm〜(2)之间,平均值为45,172.17Ωm〜(2)。纵向电导S在0.001至0.221之间,平均值为0.036。洪泛区的导水率介于0.21 m / day至29.06 m / day之间,平均值为11.22 m〜(2)/ day。各个层获得的透射率值在1.68 m〜(2)/天至808.16 m〜(2)/天之间,平均值为214.07 m〜(2)/天。在洪泛区上划定了三个地下水潜在区。液压头的结果表明,洪泛区的水位高于河流,并为河流补给水。

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